Dwr. Wallace, ANTHROPOGENIC CHLOROFLUOROMETHANES AND SEASONAL MIXING RATES IN THE MIDDLE ATLANTIC BIGHT, Deep-sea research. Part 2. Topical studies in oceanography, 41(2-3), 1994, pp. 307-324
Measurements of the chlorofluorocarbons (CFCs), F11 (CCl3F) and F12 (C
Cl2F2) were made during the Shelf Edge Exchange Processes II (SEEP-IT)
experiment in the Middle Atlantic Eight during 1988-1989. These compo
unds undergo large seasonal variations in surface water concentration
as a result of temperature-induced solubility changes. Outgassing in s
ummer produces vertical concentration gradients that can be exploited
to estimate a cross-pycnocline vertical eddy-diffusivity suitable for
biogeochemical flux calculations. Model results based on an explorator
y study suggest an average K-2 of 1 x 10(-5) m(2) s(-1) for this regio
n during the stratified period. CFCs have advantages over other budget
approaches for studying mixing processes, including heat budgets, as
there are no internal sources or sinks other than air-sea gas exchange
. In order to exploit further the CFC budget of sub-pycnocline shelf w
aters, regular cruises through the summer months and characterization
of CFC levels at the time of stratification are required.